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dc.contributor.authorPérez López, Raúl
dc.contributor.authorMoragas-Segura, Natalia
dc.contributor.authorElez Villar, Javier 
dc.contributor.authorSilva Barroso, Pablo Gabriel 
dc.contributor.authorGiner Robles, Jorge
dc.contributor.authorRodríguez Pascua, Miguel Ángel
dc.contributor.authorRamos, Adrià
dc.contributor.authorPerucha, María Ángeles
dc.contributor.authorRoquero, Elvira
dc.contributor.authorGarduño-Monroy, Víctor H.
dc.date.accessioned2025-12-19T09:16:01Z
dc.date.available2025-12-19T09:16:01Z
dc.date.issued2024-04-11
dc.identifier.citationPérez-López, R., Moragas-Segura, N., Elez, J., Silva, P. G., Giner-Robles, J. L., Rodríguez- Pascua, M. A., Ramos, A., Perucha, M. A., Roquero, E., and Garduño-Monroy, V. H. (2024). Teotihuacan ancient culture affected by megathrust earthquakes during the early Epiclassic Period (Mexico). Journal of Archaeological Science Reports 55, 104528. https://doi.org/10.1016/j.jasrep.2024.104528es_ES
dc.identifier.issn2352-409X
dc.identifier.urihttp://hdl.handle.net/10366/168409
dc.description.abstract[EN]Teotihuacan was one of the thriving cultures in the Mesoamerica pre-Hispanic times, located in the Central Valley of Mexico. The city-state was a dominant centre point during the Classic period and its influence affected other contemporaneous cultures. Around the year 550 CE, a continuous decrease in urban population and selective building destruction was noted, accompanied by widespread fire. The layout of the city is identified by an avenue that articulates the political-administrative and religious centres, with such significant and impressive buildings as the Pyramid of the Sun, the Pyramid of the Moon and the Temple of Feathered Serpent. A systematic analysis of building damage in the pyramids reveals several Earthquake Archaeological Effects, (EAEs) potentially related to seismic loading. A damage pattern compatible with a strong ground shaking was also identified in the west staircase of the Old Temple of the Feathered Serpent, in the first rows of the west staircase of the Adosada platform (New Temple), and in the Pyramid of the Sun. In total, five ancient earthquakes have been determined from the damage, dated from the Tzacualli cultural period (1–100 CE), to the Xolalpan – Metepec period (450–550 CE). Unfortunately, this methodology does not determine the earthquake source. Therefore, we consider the possibility that repetitive megathrust earthquakes (Mw > 8.5) from the Middle American Trench (Pacific coast) could be responsible for the spatial pattern of the building damage. This proposal does not conflict with other existing theories for the Teotihuacan abrupt collapse, considering that the sudden overlapping of natural disasters like earthquakes could increase internal warfare (uprising), and civil unrest.es_ES
dc.description.sponsorshipInstituto Geológico y Minero de España (IGME-CSIC) This work was supported by the Project FAMRAD (PID2020-113407RB-I00) and is part of the research activities of PID2021- 123510OB-I00 (USAL) AEI/10.13039/501100011033/ of the Spanish Ministry of Science; the Program Lost Cities funded by the Gerda Henkel Foundation (AZ 02/LC/20).es_ES
dc.format.mimetypeapplication/pdf
dc.language.isoenges_ES
dc.publisherElsevier Ltd.es_ES
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectArchaeoseismologyes_ES
dc.subjectEarthquakees_ES
dc.subjectTeotihuacanes_ES
dc.subjectMexicoes_ES
dc.subject.meshGeological Processes *
dc.subject.meshGeological Phenomena *
dc.subject.meshGeology *
dc.titleTeotihuacan ancient culture affected by megathrust earthquakes during the early Epiclassic Period (Mexico)es_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.relation.publishversionhttps://doi.org/10.1016/j.jasrep.2024.104528es_ES
dc.subject.unesco2506.20 Geología Estructurales_ES
dc.subject.unesco2506 Geologíaes_ES
dc.subject.unesco2507.05 Sismología y Prospección Sísmicaes_ES
dc.identifier.doi10.1016/j.jasrep.2024.104528
dc.relation.projectIDPID2020-113407RB-I00 (FAMRAD)es_ES
dc.relation.projectIDPID2021- 123510OB-I00 (QTECTIBERIA - USAL)es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.journal.titleJournal of Archaeological Science: Reportses_ES
dc.volume.number55es_ES
dc.page.initial104528es_ES
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones_ES
dc.subject.decsprocesos geológicos *
dc.subject.decsfenómenos geológicos *
dc.subject.decsgeología *


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